Permo-Triassic anatexis, continental rifting and the disassembly of western Pangaea
Crustal anatectites are frequently observed along ocean–continent active margins, although their origins are disputed with interpretations varying between rift-related and collisional. We report geochemical, isotopic and geochronological data that define an ~ 1500 km long belt of S-type meta-granite...
Published in: | Lithos |
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Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2014
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Subjects: | |
Online Access: | https://archive-ouverte.unige.ch/unige:34028 |